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Peridotite Enclaves Hosted by Mesoarchaean TTG-Suite Orthogneisses in the Fiskefjord Region of Southern West Greenland ⇑ Kristoffer Szilas A,B, , Peter B

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Peridotite Enclaves Hosted by Mesoarchaean TTG-Suite Orthogneisses in the Fiskefjord Region of Southern West Greenland ⇑ Kristoffer Szilas A,B, , Peter B GeoResJ 7 (2015) 22–34 Contents lists available at ScienceDirect GeoResJ journal homepage: www.elsevier.com/locate/GRJ Peridotite enclaves hosted by Mesoarchaean TTG-suite orthogneisses in the Fiskefjord region of southern West Greenland ⇑ Kristoffer Szilas a,b, , Peter B. Kelemen c, Stefan Bernstein d a Department of Geological & Environmental Sciences, Stanford University, 450 Serra Mall, Stanford, CA 94305, USA b Faculty of Science, University of Southern Denmark, Campusvej 55, 5230 Odense, Denmark c Lamont-Doherty Earth Observatory, Columbia University, PO Box 1000, Palisades, NY 10964, USA d Avannaa Resources, Dageløkkevej 60, 3050 Humlebæk, Denmark article info abstract Article history: This study presents bulk-rock major, trace, and platinum-group element data, as well as mineral chem- Received 27 December 2014 istry for peridotites which form large enclaves (up to 500 Â 1000 m) within Mesoarchaean orthogneisses Revised 30 March 2015 of the Akia terrane in the Fiskefjord region, southern West Greenland. The largest peridotite body, known Accepted 31 March 2015 as Seqi, contains highly fosteritic olivine with a median Mg# of 92.6 and hosts extensive layers of chromi- tite, which can be traced for tens of metres with thicknesses of up to 30 cm. Thinner (<100 m thick), but extensive (up to 2000 m long) peridotite sheets are associated with coarse norite and orthopyroxenite Keywords: with distinct cumulate textures in the Amikoq complex, located a few tens of kilometres south of Seqi. Ultramafic cumulate Intercalated amphibolites of tholeiitic basaltic composition show complementary geochemical evolution Seqi Amikoq to the peridotites, consistent with igneous crystal fractionation trends. The U-shaped trace element pat- Platinum-group elements terns of the peridotites may either reflect the parental melt composition from which these olivine-rich Norite rocks were derived, or alternatively this feature may be the result of melt-rock interaction. Overall, we Orthopyroxenite interpret the Fiskefjord region peridotites to have formed as ultramafic cumulates derived from Archaean high-Mg, low Ca/Al magmas, although their geodynamic setting remains to be established. Ó 2015 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). 1. Introduction peridotites in the Amikoq complex (Fig. 1). The tholeiitic basaltic rocks and are similar to the amphibolites from other supracrustal Peridotites are found sporadically as large enclaves within belts in the North Atlantic craton. Although the field relations Mesoarchaean amphibolite- to granulite-facies orthogneisses in between these mafic and ultramafic rocks are not clear, they appear the Akia terrane of southern West Greenland, North Atlantic craton to be part of the same rock association, which includes the Qussuk [39]. These peridotites consist mainly of chromite-rich dunite and and Bjørneøen supracrustal belts [39,40]. minor harzburgite. They commonly contain amphibole, but essen- Two contrasting origins can be envisioned for the Fiskefjord tially no clinopyroxene is observed. Although the Seqi dunite body, region peridotites: Either they represent (1) residual mantle resi- which is the largest of the ultramafic enclaves at ca. 500 Â 1000 m, dues formed by large degrees of melt-extraction, or (2) alterna- has been mined for industrial grade olivine, the origin of these peri- tively they represent ultramafic cumulates formed by mainly dotites is yet unknown. These unusually large inclusions of coarse olivine accumulation (+spinel ± orthopyroxene). If these peridotites found within tonalite–trondhjemite–granodiorite peridotites were originally mantle residues then these mafic to (TTG)-suite orthogneisses, are not a common feature of other ultramafic rock assemblages may represent remnants of ophiolitic Archaean cratons. The only similar cases occur where layered mafic crust that was obducted during accretionary processes. intrusions are present (e.g., Stillwater and Bushveld). However, all Accordingly, this would suggest that horizontal tectonics were in of the Fiskefjord peridotites are intruded by the TTGs and thus pre- operation prior to 3000 Ma. This is currently a much debated topic date the continental crust-forming event of the Akia terrane at ca. and the apparent absence of mantle rocks associated with 3000 Ma. Mafic amphibolites and norites are intercalated with the Archaean supracrustal belts is a critical point in the arguments for and against Archaean subduction zone processes (see Discussion of [12,120,121]). ⇑ Corresponding author at: Department of Geological & Environmental Sciences, Stanford University, 450 Serra Mall, Stanford, CA 94305, USA. On the other hand, if these peridotites rather formed during E-mail address: [email protected] (K. Szilas). fractional crystallisation and cumulate processes, this could have http://dx.doi.org/10.1016/j.grj.2015.03.003 2214-2428/Ó 2015 The Authors. Published by Elsevier Ltd. This is an open access article under the CC BY-NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/). K. Szilas et al. / GeoResJ 7 (2015) 22–34 23 Fig. 1. Geological map of the Nuuk and Fiskefjord regions in southern West Greenland. The peridotite locaties of the Seqi Olivine Mine and the Amikoq complex, from which the studied samples have been collected, are shown in purple. Two additional large peridotite bodies (Miaggoq and Ulamertoq) are present, but no samples are currently available from these localities. The map in based on work by the Geological Survey of Denmark and Greenland (GEUS). important economic implications, given that Ni and platinum- inference is supported by the observation of a similar intimate group element (PGE) mineralisation is typically hosted by ultra- association of these particular lithologies at the Miaggoq and mafic cumulates e.g., [82,77]. In either case, these peridotites and Ulamertoq localities. However, no data is presently available from the associated norites, orthopyroxenites, and mafic supracrustal these two peridotite bodies. rocks, which are also found as related belts and slivers within these The Nuuk region consists of several discrete crustal terranes, TTG-suite orthogneisses, may yield important new insights into with the oldest being the over 3600 Ma Itsaq gneiss complex the crustal evolution of the North Atlantic craton. In this [87], that were ultimately amalgamated during the Neoarchaean contribution bulk-rock and mineral geochemical data for the peri- [34,86]. A recent study by Dziggel et al. [29] interpreted this region dotites are presented with the aim of elucidating the petrogenesis as comprising paired metamorphic belts, implying that the of the ultramafic components of the Akia terrane. amalgamation occurred in an accretionary setting. Peridotites are also reported within the Itsaq gneiss complex, but these are not 2. Regional geology as extensive as those of the Akia terrane and appear to be directly associated with anorthosite and gabbro. Thus, the peridotites of the Fiskefjord is located in the northern part of the Nuuk region and Nuuk and Akia terranes appear to be of different origins cuts through Mesoarchaean orthogneisses of the Akia terrane. The [14,36,98,97]. A recent overview of the igneous and metamorphic present study describes peridotites found along the Fiskefjord, as history of the Akia terrane can be found in Garde et al. [43]. well as at the Seqi and the Amikoq localities to the north and south, Below we outline the main geological features that are relevant respectively (Fig. 1). At the Amikoq locality, the peridotites crop for understanding the Fiskefjord region peridotites. out together with intercalated norites and orthopyroxenites, which The regional TTG-suite orthogneisses of the Akia terrane, which based on their close association, appear to be co-genetic [39]. This host the Seqi-Amikoq association of peridotites and supracrustal 24 K. Szilas et al. / GeoResJ 7 (2015) 22–34 rocks, have been dated by U-Pb in zircon at ca. 3050–3000 Ma of rocks are distinguished, namely (1) dunites from the Seqi Olivine [39,40]. Subordinate dioritic gneisses have magmatic ages of about Mine and (2) various types of peridotites found along Fiskefjord 3200 Ma, and represent local pre-existing crust [39]. The amphibo- and in the Amikoq complex. Throughout this study, the latter lite-facies supracrustal rocks that are present within the Akia two areas are collectively referred to as the ‘Fiskefjord orthogneisses have been dated directly at ca. 3071 Ma using mag- peridotites’, whereas the term ‘Fiskefjord region peridotites’ is used matic zircon extracted from a volcano-sedimentary schist found for all of these rocks including the Seqi dunites. within the mafic to andesitic Qussuk–Bjørneøen volcanic sequence The peridotites from the Seqi Olivine Mine are dominated by [40]. Aluminous schists present in the Qussuk sequence have been dunites, whereas the Fiskefjord peridotites comprise both dunites proposed to represent metamorphosed hydrothermally altered and amphibole-bearing harzburgites. The latter are commonly basalt [41]. Such lithologies are also present within the Amikoq associated with norites, and minor orthopyroxenite layers are also complex [2], and are also found in the Storø supracrustal belt about present. However, the focus of the present study is exclusively on 10 km southeast of the Qussuk peninsula [104,110]. Leucocratic the geochemistry of the peridotites, and we rely on previously fragmental
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